Pen Allt-mawr

Pen Allt-mawr is a 719 metres (2,359 ft) high subsidiary summit of Waun Fach and the third highest peak in the Black Mountains in south-eastern Wales. A very recognisable and prominent peak of the Black Mountains, it lies near the end of the more westerly of Waun Fach's two broad southern ridges. Its top Pen Twyn Glas is to the north, while its close neighbour Pen Cerrig-calch is to the south.[1] A prominent spur 1km to the SSW of the summit is known as Pen Gloch-y-pibwr. The stepped Bryniog ridge curves southward from this point.

Pen Allt-mawr
Pen Allt-mawr from Pen Cerrig-calch
Highest point
Elevation719 m (2,359 ft)
Prominence102 m (335 ft)
Parent peakWaun Fach
ListingHewitt, Nuttall, HuMP
Coordinates51.9118°N 3.1544°W / 51.9118; -3.1544 
Naming
English translationtop of the big slope
Language of nameWelsh
Geography
LocationBlack Mountains, South Wales
OS gridSO206243
Topo mapOS Landranger 161
Listed summits of Pen Allt-mawr
NameGrid refHeightStatus
Pen Twyn GlasSN969193646 metres (2,119 ft)sub Hewitt, Nuttall

Its summit is stony and has damaged Bronze Age cairns and a large shelter cairn together with a trig point.[2] Further Bronze Age cairns are found along the western edge of the plateau to the south.

Geology

The summit of Pen Allt-mawr is at the northern tip of a broadly triangular summit surface formed from a slab of southerly tilting upper Old Red Sandstone traditionally known as the Quartz Conglomerate. These rocks which date from the Late Devonian Epoch are continuous with those of Pen Cerrig-calch but other than a tiny outlier forming the summit of Sugar Loaf, are found nowhere else within the Black Mountains. Beneath the Quartz Conglomerate are the Early Devonian sandstones of the Brownstones Formation which form the upper slopes and summits of Pen Twyn Glas and Mynydd Llysiau to the north (though are barely seen). More readily eroded mudstone bands within this formation give rise to the stepped appearance of this hill and many of its neighbours. Sandstones of the Senni Formation (traditionally the 'Senni Beds') form the lower slopes of the mountain.[3]

gollark: "Genius" is far too underwhelming a word to capture our sheer intellect, yes.
gollark: According to me™, stuff is vaguely okay, and by many metrics appears to be improving.
gollark: ···.
gollark: Faster, though.
gollark: If I was forced to write all osmarks.net backend services as highly optimized C or something, they would probably be buggier, slower, less maintainable and lacking features.

References
  1. Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. ISBN 1-85284-304-7.
  2. "Pen Alltmawr cairn II". Coflein. RCAHMW. Retrieved 17 May 2020.
  3. "England and Wales sheet 214 'Talgarth'". Maps portal. British Geological Survey. Retrieved 17 May 2020.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.